A new paper has been accepted for publication in the Journal of Climate titled "Quantifying climate change in the tropical mid troposphere over East Africa from glacier shrinkage on Kilimanjaro" with authors Thomas Mölg, Nicolas Cullen, Douglas Hardy, Michael Winkler, and Georg Kaser. This group has been collaborating for several years; most are part of the Tropical Glaciology Group at the Univerity of Innsbruck.
The paper examines 19th century recession of the southern-slope Kersten Glacier, by backward modeling with a spatially-distributed mass-balance model. Results indicate that late-19th century precipitation was higher by +160 to +240 mm/yr, dominating the mass budget and producing a larger glacier extent. Today, the Kersten Glacier terminus is ~600 m higher in elevation, and the glacier is loosing mass at ~500 kg/m^2/yr.
-Doug Hardy, UMass Geosciences
Wednesday, April 15, 2009
Friday, April 10, 2009
Another dry month
Little snowfall on the Northern Ice Field between mid-February and 28 March, satellite telemetry indicates. Only one mid-month event of 2 cm. Then, a snowy interval 28 March to 2 April bringing ~6 cm of accumulation. Six centimeters isn't much, but it is enough to substantially raise the albedo and keep it elevated for several weeks. Hopefully more snow will follow...
-Doug Hardy, UMass Geosciences
-Doug Hardy, UMass Geosciences
Wednesday, April 8, 2009
2009 Long Rains...
seem to be late. Normally, the wet season is underway by now. Through most of March this year, however, conditions remained dry. Very soon we will post a synopsis of measurements on the weather page. Normally this page is updated on the first or second of each month, but we're late this month due to personnel changes in the UMass Climate Center.
Monday, March 30, 2009
Still dry - mid-February
"light dusting of snow" at the summit (1-3 cm), February 16
- Hassan Basagic, Portland State University
- Hassan Basagic, Portland State University
Sunday, February 1, 2009
January fieldwork

No such luck. The 2008 short rains utterly failed, both on the mountain and regionally. In conjunction with conflict earlier in the year, this lack of rainfall brought great hardship to eastern Kenya. By mid-January, Kibo's summit had not seen subsantial snowfall since early June, so very low surface albedo was causing considerable absorption of solar radiation. The impact? Mass loss from horizontal ice surfaces - lots of it! Satellite telemetry from the station revealed a grim reality, that measurements were in jepeordy without a trip to reset (lower) the tower down into the ice (cf. New York Times, Feb. 2001).
Fortunately, collaborators from Innsbruck had been planning a January 2009 trip for several months, and were kind enough to let me piggy-back onto their logistics. This trip was based from the Marangu Hotel's peaceful setting, and their staff supported our effort on the mountain. We spent only 4 nights going up, a bit less than I've found optimal, and then 3 at the summit.
No snow was visible on the mountain from Marangu, or from the east side as we drove around to Rongai - conditions more typical of August. Thereafter though, every day of our trip featured rain and/or snow and/or thunder, except, paradoxically, our final descent through the rainforest.
At the summit, ablation since September was readily apparent. A thin mantle of new snow (5-10 cm, accumulating daily) partially obscurred dirtier ice surfaces than I'd seen in years (see image above). Some horizontal ice surfaces are now quite old (decades to centuries), with high dust concentrations causing low albedo. In just 4 months, ablation had reduced ice thickness by a meter in some places! On one glacier, 7 of 8 mass balance stakes had ablated out, and drilling new holes on 3 different glaciers occupied a chunk of my time. However, work focused on lowering the tower; most of the job was done in just over 2 strenuous hours, thanks to help from Geoffry, Good Luck, Leoned, David and Samuel.
Descending from the summit glaciers in a snowstorm, we pondered whether the short rains were late in arriving, or the long rains were beginning early.
-Doug Hardy, UMass Geosciences
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